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Lithuanian karst region rivers' water ecology: hydrochemical and hydrobiological evaluation

机译:立陶宛喀斯特地区河流水生态学:水化学和水生物评价

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The Lithuanian karst region covers about 1000 km~3 in the northern part of the country. This is the most vulnerable area from a pollution point of view. The structure of the total dissolved solids (TDS) shows that the flow of rivers in the karst region is from hydraulically interconnected aquifers. For the last decade (1991―2000) TDS has varied considerably, from 529 to 732 mg/l. The predominant sources of nitrogen and phosphorus within the headwaters of the monitored rivers were diffuse and agricultural in nature. Downstream from the towns nitrogen and especially phosphorus showed both diffuse and point source signals. Contributions of point sources to the stream pollution by nutrients prevail. The time series of monthly dissolved oxygen (O_2) in the main karst region river ― the Musa ― shows the existence of multiplicative seasonality. The trend cycle (1991 -1999) shows low levels of dissolved oxygen in 1991 ―1993, with a similar fluctuation in 1994, 1995 and 1996 (due to point pollution from the town of Siauliai) and a gradually improving situation since 1997. The general multiplicative trend of dissolved oxygen in the lower reaches of the Musa river (near the border with Latvia) is decreasing (within the accuracy limits). The abundance and species of zoo benthos are suitable criteria (biotic index ― Bl) for evaluation of a river's biological water quality. Zoo benthos demonstrates tolerances that vary among species, the oxygen regime and the pollution with nitrogen. The best living conditions for invertebrates are in the riverhead of the karst region rivers ― Bl = 5.62-6.74 (1991 ― 1999), where pollution with nutrients is caused mostly by agricultural activity. Rare and asynchronous data of biological water quality shows up tendencies that invertebrates prefer less contaminated reaches of rivers.
机译:立陶宛喀斯特地区在该国北部约1000 km〜3。从污染的角度来看,这是最脆弱的地区。总溶解固体(TDS)的结构表明,喀斯特地区的河流来自水力连通的含水层。在过去十年(1991年至2000年)中,TDS发生了很大变化,从529毫克/升至732毫克/升。被监测河流上游水源中的氮和磷的主要来源是分散的,并且具有农业性质。在城镇的下游,氮,尤其是磷同时显示了扩散和点源信号。点源对养分对河流污染的贡献占主导。喀斯特地区主要河流穆萨河中每月溶解氧(O_2)的时间序列表明存在乘性季节性。趋势周期(1991年至1999年)显示,1991年至1993年的溶解氧水平较低,1994年,1995年和1996年的波动幅度相似(由于希奥利艾镇的点污染),自1997年以来情况逐渐改善。穆萨河下游(与拉脱维亚接壤的边界附近)的溶解氧的乘积趋势正在减小(在精度范围内)。动物园底栖动物的丰富度和种类是评估河流生物水质的合适标准(生物指数― Bl)。动物园的Bentos表现出的耐受性因物种,氧气状况和氮污染而异。无脊椎动物的最佳生活条件是在喀斯特地区河流的河口-Bl = 5.62-6.74(1991-1999),那里的养分污染主要是由农业活动造成的。生物水质量的稀有和异步数据表明,无脊椎动物更喜欢受污染较小的河流。

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